喜马拉雅康巴淡色花岗岩的高分异成因及 岩浆⁃热液演化特征

刘志超, 刘小驰, 俞良军, 王建刚

Highly fractionated origin and magmtic⁃hydrothermal evolution of the Kampa leucogranites in the Tethyan Himalaya

Zhichao Liu, Xiaochi Liu, Liangjun Yu, Jian'gang Wang

图10 康巴淡色花岗岩的Zr/Hf,Nb/Ta,Y/Ho和K/Rb比值以及与TE1,3相关关系特征 (The data for the continental crust is after ref.[34],the fields of the CHARAC are after ref.[33,35])

Fig. 10 Variations of Zr/Hf,Nb/Ta,Y/Ho and K/Rb versus TE1,3 of the Kamba leucogranite